atmoslapse
Use Lapse Rate Atmosphere model
Syntax
Description
[
implements the mathematical representation of the lapse rate atmospheric equations for
ambient temperature, speed of sound, pressure, and density for the input geopotential
altitude. To customize this atmospheric model, specify the atmospheric properties in the
function input. T
,a
,P
,rho
]
= atmoslapse(height
,g
,heatRatio
,characteristicGasConstant
,lapseRate
,heightTroposphere
,heightTropopause
,density0
,pressure0
,temperature0
)
[
indicates that the values for ambient temperature, speed of sound, pressure, and density are
for below mean sea level geopotential altitudes.T
,a
,P
,rho
]
= atmoslapse(height
,g
,heatRatio
,characteristicGasConstant
,lapseRate
,heightTroposphere
,heightTropopause
,density0
,pressure0
,temperature0
,height0
)
The function holds temperature and pressure values below the geopotential altitude of
height0
and above the geopotential altitude of the tropopause. The
function calculates the density and speed of sound using a perfect gas relationship.
[
implements the mathematical representation of the lapse rate atmospheric equations for
ambient temperature, speed of sound, pressure, density, kinematic viscosity, and dynamic
viscosity for the input geopotential altitude. Density and speed of sound are calculated
using a perfect gas relationship. Viscosity is computed using Sutherland's formula for ideal
gas.T
,a
,P
,rho
,nu
,mu
]
= atmoslapse(height
,g
,heatRatio
,characteristicGasConstant
,lapseRate
,heightTroposphere
,heightTropopause
,density0
,pressure0
,temperature0
,height0
,Name=Value
)
Examples
Input Arguments
Output Arguments
References
[1] U.S. Standard Atmosphere. Washington, DC: US Government Printing Office, 1976.
Version History
Introduced in R2006bSee Also
atmoscira
| atmoscoesa
| atmosisa
| atmosnonstd
| atmospalt